英语翻译另外,泥岩还承受比上部各土层更多的上覆荷载,需要加入(或排除)压力对水的冻结温度以及未冻水含量的影响.水的冻结温

英语翻译
另外,泥岩还承受比上部各土层更多的上覆荷载,需要加入(或排除)压力对水的冻结温度以及未冻水含量的影响.水的冻结温度和压力存在如下关系式[29]:
(MPa) (2-14)
而张立新(1998)的试验结果也证实冻土的冻结温度随压力的增大而呈现线性地降低,其斜率接近于–0.075℃∕MPa[30].根据公式2-14,水的冻结温度降低0.1℃(即Tm=273.05 K)时,其所需压力1.397 MPa.而由文[30]计算得,冻土冻结温度降低0.1 ℃所需压力为1.33 MPa.两者在数量上接近,一方面相互验证了结果的正确性,另一方面也说明冻土在压力作用下冻结温度的降低主要是由水的冰点降低造成的.根据岩芯资料计算,要达到上述压力,土体的深度要超过50 m.所以,压力对未冻水含量的影响在本文中就不再考虑了.
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烂菜 1年前 已收到1个回答 举报

wangfeiyan 幼苗

共回答了17个问题采纳率:94.1% 举报

In addition, the mudstoen bears more cover load than that of soil layer, so the effect of pressure upon water freezing temperature and unfrozen water content should be considered (or eliminated).
The formula of water freezing temperature and pressure is as follow:
(MPa) (2-14)
But, the test result by Zhang Lixin (1998) also approved that the freezing temperature of frozen soil increases as the pressure decreases, its gradient is close to -0.075℃/MPa [30].
According to formula 2-14, the water freezing temperature drops 0.1℃ (that is at Tm=273.05K), its pressure needed is 1.397MPa.
Knowing from the calculation [30], the freezing temperature of frozen soil drops 0.1 ℃ and its pressure needed is 1.397MPa.
Both are close quantitatively, and both result, on the one hand, were validated each other, and on the other hand it was illustrated that the freezing temperature drop of frozen soil tempertaure activated by of pressure was caused by the drop of water freezing temperature.
According to the core calculation, in order to obtain the said pressure, the depth of soil body should be over 50 meters. So, the effect of pressure on unfrozen water content is not considered in this paper.

1年前

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